矿区山前钾化带是钾化蚀变的产物，局部地段构成矿体。
Piedmont potassic alteration zone is the product of potash feldspathization, part of the zone is ore body.
该区域的主要勘探目标是，含有钙质结砾岩和钒钾铀矿砾岩石单元的水系，这些岩石赋存着含有钒钾铀矿的次生矿化带。
The principal exploration target for the area is the drainage system that contains the calcrete and silcrete units that host the carnotite-bearing secondary uranium mineralisation.
从中心向外依次为钾硅酸盐化带、石英绢云母化带、青磐岩化带。
The concentric alteration zones from the inner outward are successively the K-silicate zone, the quartz-sericite zone, and the propylitic zone.
从中心向外依次为钾硅酸盐化带、石英绢云母化带、青磐岩化带。
The concentric alteration zones from the inner outward are successively the K-silicate zone, the quartz-sericite zone, and the propylitic zone.
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